This article reviews the geology of the Sveconorwegian orogen in south Scandinavia and
existing tectonic models for the Mesoproterozoic to Neoproterozoic Sveconorwegian …

Abstract Long-lived (800 Ma) Paleo–to Mesoproterozoic accretionary orogens on the
margins of Laurentia, Baltica, Amazonia, and Kalahari collided to form the core of the …

This paper presents a plate-scale model for the Precambrian growth and evolution of the
North American continent. The core of the North American continent (Canadian shield) came …

A total of 4344 magmatic U-Pb ages in the range 2300 to 800 Ma have been compiled from
the Great Proterozoic Accretionary Orogen along the margin of the Columbia/Nuna …

To this day, there is a great amount of controversy about where, when and how the so-called
supercontinents--Pangea, Godwana, Rodinia, and Columbia--were made and broken …

The origin and tectonic setting of the Mesoproterozoic (1.50–1.34 Ga) granite–rhyolite
Provinces of the midcontinent region of the United States, and the coeval A-type granite …

The Chinese Altai orogen is a typical domain of the Central Asian Orogenic Belt and in
previous syntheses was divided into six tectonic units (or terranes). In this paper, 41 new …

In recent years, a rapidly expanding database, especially in sensitive high-resolution ion
microprobe (SHRIMP) geochronology, has led to significant advances in understanding of …

This paper presents new geochronologic, isotopic, and geochemical data bearing on the
evolution of Proterozoic crust in SW Mato Grosso state, Brazil, which is at the southern end …

Zircon age peaks at 2100–1650 and 1200–1000 Ma correlate with craton collisions in the
growth of supercontinents Nuna and Rodinia, respectively, with a time interval between …